Enthalpy Relaxation Phenomenon in a Heavy Ice Crystal
Abstract The heat capacities of quenched and annealed heavy ice Ih were measured in the temperature range 14 to 300 K by an adiabatic calorimeter. A relaxational thermal anomaly was found at around 115 K and this phenomenon was ascribed to the onset of deuteron ordering in the crystal. The average a...
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Cambridge University Press (CUP)
1978
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crcambridgeupr:10.1017/s0022143000033931 2024-03-03T08:45:57+00:00 Enthalpy Relaxation Phenomenon in a Heavy Ice Crystal Haida, Osamu Suga, Hiroshi Seki, Syūzō 1978 http://dx.doi.org/10.1017/s0022143000033931 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000033931 en eng Cambridge University Press (CUP) Journal of Glaciology volume 21, issue 85, page 707 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1978 crcambridgeupr https://doi.org/10.1017/s0022143000033931 2024-02-08T08:36:10Z Abstract The heat capacities of quenched and annealed heavy ice Ih were measured in the temperature range 14 to 300 K by an adiabatic calorimeter. A relaxational thermal anomaly was found at around 115 K and this phenomenon was ascribed to the onset of deuteron ordering in the crystal. The average activation enthalpy of the relaxational process was determined to be (26±5) kJ mol -1 . Residual entropies of the crystal were recalculated on the basis of the present heat-capacity data combined with the revised values for enthalpy of vaporization, saturated vapour pressure, and spectroscopic entropy. They are (3.47±0.41 J K -1 mol -1 for the quenched crystal and (3.44±0.41) J K -1 mol -1 for a crystal annealed at 102-106 K for 264 h. The characteristics and the origin of the anomaly are discussed in comparison with that of ordinary ice. This paper has been accepted for publication in full in a forthcoming issue of the Journal of Glaciology . Article in Journal/Newspaper Journal of Glaciology Cambridge University Press Journal of Glaciology 21 85 707 |
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Open Polar |
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Cambridge University Press |
op_collection_id |
crcambridgeupr |
language |
English |
topic |
Earth-Surface Processes |
spellingShingle |
Earth-Surface Processes Haida, Osamu Suga, Hiroshi Seki, Syūzō Enthalpy Relaxation Phenomenon in a Heavy Ice Crystal |
topic_facet |
Earth-Surface Processes |
description |
Abstract The heat capacities of quenched and annealed heavy ice Ih were measured in the temperature range 14 to 300 K by an adiabatic calorimeter. A relaxational thermal anomaly was found at around 115 K and this phenomenon was ascribed to the onset of deuteron ordering in the crystal. The average activation enthalpy of the relaxational process was determined to be (26±5) kJ mol -1 . Residual entropies of the crystal were recalculated on the basis of the present heat-capacity data combined with the revised values for enthalpy of vaporization, saturated vapour pressure, and spectroscopic entropy. They are (3.47±0.41 J K -1 mol -1 for the quenched crystal and (3.44±0.41) J K -1 mol -1 for a crystal annealed at 102-106 K for 264 h. The characteristics and the origin of the anomaly are discussed in comparison with that of ordinary ice. This paper has been accepted for publication in full in a forthcoming issue of the Journal of Glaciology . |
format |
Article in Journal/Newspaper |
author |
Haida, Osamu Suga, Hiroshi Seki, Syūzō |
author_facet |
Haida, Osamu Suga, Hiroshi Seki, Syūzō |
author_sort |
Haida, Osamu |
title |
Enthalpy Relaxation Phenomenon in a Heavy Ice Crystal |
title_short |
Enthalpy Relaxation Phenomenon in a Heavy Ice Crystal |
title_full |
Enthalpy Relaxation Phenomenon in a Heavy Ice Crystal |
title_fullStr |
Enthalpy Relaxation Phenomenon in a Heavy Ice Crystal |
title_full_unstemmed |
Enthalpy Relaxation Phenomenon in a Heavy Ice Crystal |
title_sort |
enthalpy relaxation phenomenon in a heavy ice crystal |
publisher |
Cambridge University Press (CUP) |
publishDate |
1978 |
url |
http://dx.doi.org/10.1017/s0022143000033931 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000033931 |
genre |
Journal of Glaciology |
genre_facet |
Journal of Glaciology |
op_source |
Journal of Glaciology volume 21, issue 85, page 707 ISSN 0022-1430 1727-5652 |
op_doi |
https://doi.org/10.1017/s0022143000033931 |
container_title |
Journal of Glaciology |
container_volume |
21 |
container_issue |
85 |
container_start_page |
707 |
_version_ |
1792501651543687168 |